
mineral
Quartz (Milky Quartz)
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: White to opaque; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- White to opaque
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: White to opaque; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the cooling of silica-rich magma or from hydrothermal veins. Milky quartz gets its appearance from tiny fluid inclusions of gas or liquid trapped during crystal growth. They are found across all geological ages.
Uses & applications
Used in glassmaking, electronics (piezoelectric properties), abrasives, construction aggregates, and as a semi-precious gemstone in jewelry.
Geological facts
Quartz is the most abundant and widely distributed mineral found at Earth's surface. Milky quartz is the most common variety of crystalline quartz.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), lack of cleavage, and white opaque color. Commonly found in gravel, stream beds, and mountainous regions worldwide.
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